| This core appears in the following publications: | ||
| Cofaigh, Colm {\'O} and Davies, Bethan J and Livingstone, Stephen J and Smith, James A and Johnson, Joanne S and Hocking, Emma P and Hodgson, Dominic A and Anderson, John B and Bentley, Michael J and Canals, Miquel and others Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2014.06.023 |
Cores in this publication |
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| Pudsey, Carol J and Evans, Jeffrey First survey of Antarctic sub--ice shelf sediments reveals mid-Holocene ice shelf retreat Geology, 2001 DOI: 10.1130/0091-7613(2001)029<0787:FSOASI>2.0.CO;2 |
Cores in this publication |
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| Core-related info: | ||
| Core name | VC275 | |
| Setting | marine | |
| Region | Prince Gustav Channel, Eastern Antarctic Peninsula | |
| Collection date | 2000-03-11 | |
| IGSN ID | ||
| Core type | vibrocore | |
| Latitude | -64.6017 | |
| Longitude | -58.095 | |
| Water depth (m) | 453.0 | |
| Core length (cm) | 534.0 | |
| Comments | ||
| Cruise-related info: | ||
| Cruise | JR48 | |
| Ship | James Clark Ross | |
| Cruise start date | 2000-03-27 | |
| Cruise end date | 2000-04-01 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 772 | 0.0 - 0.0 | Diatom-bearing clayey silt | seasonal open-marine | acid insoluble organic matter | 6450.0 ± 40.0 |
| 776 | 47.0 - 47.0 | Diatom-bearing clayey silt | seasonal open-marine/sub-ice shelf distal from grounding line | acid insoluble organic matter | 11410.0 ± 40.0 |
| 777 | 84.0 - 84.0 | Silty clay | seasonal open-marine/sub-ice shelf distal from grounding line | acid insoluble organic matter | 14810.0 ± 50.0 |
| 773 | 107.0 - 107.0 | Silty clay | seasonal open-marine/sub-ice shelf distal from grounding line | acid insoluble organic matter | 18280.0 ± 60.0 |
| 774 | 124.0 - 124.0 | Diamicton | sub-ice shelf proximal to grounding line | acid insoluble organic matter | 22700.0 ± 70.0 |
| 775 | 176.0 - 176.0 | Diamicton | Subglacial | acid insoluble organic matter | 35470.0 ± 290.0 |
| Depth-age relationship: | ||
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| Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively. | ||
| Questions about this page: Ryan Venturelli |
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